Isostasy is the flotational balance achieved between rocks of the crust lithosphere and deeper mantle. This balance is maintained as lighter rocks of the crust "float" on the denser rocks of the mantle below.
The force responsible for the Earth's crust and lithosphere floating on the mantle is isostasy. Isostasy is a balancing act between the buoyant force of the lithosphere on the denser, more fluid asthenosphere below it. This balance helps maintain the equilibrium of the Earth's crust.
lithosphere
The region below the Earth's crust is called the mantle. It is composed of solid rock that is more rigid than the crust but less dense than the core. The mantle plays a key role in the movements of tectonic plates and the heat flow of the Earth.
The boundary between the Earth's crust and outer mantle is known as the Mohorovičić discontinuity, or Moho. It is typically located around 5 to 10 kilometers below the oceanic crust and around 20 to 90 kilometers below the continental crust. At the Moho, there is a significant increase in seismic wave velocity, indicating a change in composition and density between the crust and mantle.
Isostasy is the flotational balance achieved between rocks of the crust lithosphere and deeper mantle. This balance is maintained as lighter rocks of the crust "float" on the denser rocks of the mantle below.
The crust is above the mantle and the mantle is below the crust
Isostatic equilibrium is the balance between Earth's crust and the layer of mantle it floats on. The denser the crust is, the more it sinks into the mantle. Equilibrium is achieved when the crust floats at a certain level in the mantle.
The Earth's mantle is below the crust. The layers of the Earth form concentric spheres. Below the mantle is the core.
Mantle Is The Below Layer Of The Crust In Earth.
The force responsible for the Earth's crust and lithosphere floating on the mantle is isostasy. Isostasy is a balancing act between the buoyant force of the lithosphere on the denser, more fluid asthenosphere below it. This balance helps maintain the equilibrium of the Earth's crust.
The interior of the Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a highly viscous layer between the crust and the outer core. As such, the core (split into the solid inner and liquid outer layers) is below the mantle.
the mantle
lithosphere
15 kilo meters is the distance between the crust and the mantle
The zone between the core and crust of the Earth is the mantle. It is a layer of solid rock that extends about 1,800 miles (2,900 kilometers) below the Earth's surface. The mantle is made up of silicate minerals and is responsible for convection currents that drive plate tectonics.
the mantle